Most of the time, atmospheric rivers--plumes of lower-atmospheric moisture from off the Pacific Ocean--are relatively wide and thus produce large amounts of precipitation over a broad region.
But on Friday, something relatively unusual occurred: a very narrow "mini" atmospheric river was locked over our region for hours, producing a narrow band of intense precipitation over western Washington and into the Cascades.
You can really see it in the regional weather radar image for Friday morning (below). Yellows indicate the heaviest precipitation.
The southwest-northeast plume of heavier rain was very evident. Totally dry over the San Juans and the southern Cascades.
Consider the precipitation totals on Friday below (only values more than a third of an inch are shown).
You can clearly see the precipitation band; where the moisture plume was forced to rise by the central Cascades, 3-5 inches fell.
Local rivers have surged, some to near flood stage. The black dots below show the rivers that are now experiencing MUCH above normal flow.
The UW WRF model accurately predicted this moisture plume the day before. Below is the prediction (for Friday morning) of water vapor flux (the amount of water vapor brought in by the wind). Orange shows the highest amounts. Not bad.
Reservoir levels are moving up rapidly as a result.












Friday was kinda fun for just riding around on my bike and watching the morning unfold. The way it developed, looking at the radar Friday morning, I assumed it was a convergence zone.
ReplyDeleteIn any case, I saw more flooded steets on my bike between downtown snd Georgetown than I think I have ever seen in Seattle. Venice for a day!😅
It has certainly been a very wet month-to-date in Western Whatcom County. With nearly 5” of rain, it’s been the 6th wettest 1st half of November on record in Bellingham.
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